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中国南四湖及其主要流入河流的沉积物-水界面磷吸附特性和磷形态

Phosphate adsorption characteristics at the sediment-water interface and phosphorus fractions in Nansi Lake, China, and its main inflow rivers.

作者信息

An W C, Li X M

机构信息

College of Environmental Science and Engineering, Shandong University, Jinan 250100, People's Republic of China.

出版信息

Environ Monit Assess. 2009 Jan;148(1-4):173-84. doi: 10.1007/s10661-007-0149-6. Epub 2008 Mar 15.

DOI:10.1007/s10661-007-0149-6
PMID:18344009
Abstract

Phosphorus fractions and phosphate adsorption characteristics of 16 sediments from a shallow freshwater lake (Nansi Lake, China) and its inflow estuaries were investigated. In the present study, the sediment phosphorus is fractionated into exchangeable P (exch-P), Al-P, Fe-P, Ca-P, organic P (OP), inorganic P (IP) and total P (TP). The results show that the total phosphorus (TP) content in the sediments ranges from 571.67 to 1,113.55 mg kg(-1), and calcium bound phosphorus (Ca-P) is the main fraction of IP. The biologically available phosphorus (BAP) ranges from 32.02 to 229.67 mg kg(-1) in the Nansi Lake sediments. Phosphate adsorption on the sediments mainly occurs within 10 h and is completed within 48 h. The content of native adsorbed phosphorus (omega(NAP)) varies greatly from 6.05 to 194.37 mg kg(-1), showing a significant correlation with the total maximal amount of phosphorus adsorbed (TQ(max)). Adsorption efficiency (m) ranges from 574.79 to 3,220.68 l kg(-1) and zero equilibrium phosphorus concentration (C(EPC)) ranges from 0.010 to 0.157 mg l(-1). After the South-to-North Water Diversion Project, the inherent phosphorus present in sediments will be a major threat to the diverted water quality and be a predominant factor determining the trophic status of the lake even if the external load is reduced.

摘要

对中国南四湖及其入湖河口16个沉积物样品的磷形态和磷酸盐吸附特征进行了研究。在本研究中,沉积物中的磷被分为可交换态磷(exch-P)、铝结合态磷(Al-P)、铁结合态磷(Fe-P)、钙结合态磷(Ca-P)、有机磷(OP)、无机磷(IP)和总磷(TP)。结果表明,沉积物中总磷(TP)含量在571.67至1113.55 mg kg⁻¹之间,钙结合态磷(Ca-P)是无机磷的主要组分。南四湖沉积物中生物可利用磷(BAP)含量在32.02至229.67 mg kg⁻¹之间。沉积物对磷酸盐的吸附主要在10小时内发生,并在48小时内完成。天然吸附磷(ω(NAP))含量变化很大,在6.05至194.37 mg kg⁻¹之间,与最大吸附磷总量(TQ(max))显著相关。吸附效率(m)在574.79至3220.68 l kg⁻¹之间,零平衡磷浓度(C(EPC))在0.010至0.157 mg l⁻¹之间。南水北调工程实施后,即使外部负荷降低,沉积物中存在的内源磷仍将对调水水质构成重大威胁,并成为决定湖泊营养状态的主要因素。

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